西スマトラのサンゴに記録された海面の変化から推論された地震の超サイクル
Kerry Sieh1, Danny H Natawidjaja, Aron J Meltzner
1Tectonics Observatory, California Institute of Technology, Pasadena, CA 91125, USA. sieh@ntu.edu.sg
まとめ
メンタワイ諸島のサンゴ記録は,サンダの大気圧が200年ごとに大きな地震を引き起こすことを明らかにしています. 2007年の地震は,この地震地帯で予期されるいくつかの部分的な故障の最初のものです.
科学分野:
- 地質学 地質学 地質学
- パレオシズモロジー (Paleoseismology) とは
- テクトニクス (地質学) とは
背景:
- サンダ・メガトラストは,インドネシアにおける重要な地震活動に起因する主要な構造的特徴である.
- 大きな地震の再発間隔を理解することは,この地域の地震の危険性評価に不可欠です.
研究 の 目的:
- サンダ・メガトラストのメンタワイ部分に沿った大きな地震の歴史を再構築するために.
- このセグメントの地震の可能性と将来の破裂行動を評価する.
主な方法:
- 珊瑚の形成に保存された相対的な海面変化記録の分析.
- 珊瑚のサンプルから採取したジオクロノロジカルデータに基づく古地震再構築.
主要な成果:
- 証拠によると,過去700年間に発生した大地震は,約200年の間隔で発生している.
- 2007年のマグニチュード8.4の地震は,一連の破裂の可能性のある最初の出来事として特定されています.
結論:
- サンダ・メガトラストのメンタワイセクションは,大きな地震発生の一貫したパターンを示しています.
- 2007年の地震は,数十年にわたる部分的な故障の連続の始まりであり,継続的なモニタリングと危険性評価を必要とします.
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